Results 191 to 200 of about 13,641 (263)
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Journal of Geophysical Research: Solid Earth, 2022
Melt‐peridotite interaction is the key process causing lithological and mineralogical modification in the lithospheric mantle beneath the North China Craton (NCC). However, the lithology, kinetic, mineral, and melt compositional variations of carbonatite
X. Wang +4 more
semanticscholar +1 more source
Melt‐peridotite interaction is the key process causing lithological and mineralogical modification in the lithospheric mantle beneath the North China Craton (NCC). However, the lithology, kinetic, mineral, and melt compositional variations of carbonatite
X. Wang +4 more
semanticscholar +1 more source
Economic Geology, 2022
Carbonatite-related rare earth element (REE) deposits, the most significant source of REEs globally, are normally generated in extensional settings, such as intracontinental rifts, mantle plume-related environments, or postcollisional orogens ...
Xiaochun Li +6 more
semanticscholar +1 more source
Carbonatite-related rare earth element (REE) deposits, the most significant source of REEs globally, are normally generated in extensional settings, such as intracontinental rifts, mantle plume-related environments, or postcollisional orogens ...
Xiaochun Li +6 more
semanticscholar +1 more source
American Mineralogist, 2021
Carbonatites and related alkaline rocks host most REE resources. Phosphate minerals, e.g., apatite and monazite, commonly occur as the main REE-host in carbonatites and have been used for tracing magmatic and mineralization processes.
Jian-Hui Su +6 more
semanticscholar +1 more source
Carbonatites and related alkaline rocks host most REE resources. Phosphate minerals, e.g., apatite and monazite, commonly occur as the main REE-host in carbonatites and have been used for tracing magmatic and mineralization processes.
Jian-Hui Su +6 more
semanticscholar +1 more source
American Mineralogist, 2021
Secondary hydrothermal reworking of REEs has been widely documented in carbonatites/alkaline rocks, but its potential role in the REE mineralization associated with these rocks is currently poorly understood.
Rongtu Ma +3 more
semanticscholar +1 more source
Secondary hydrothermal reworking of REEs has been widely documented in carbonatites/alkaline rocks, but its potential role in the REE mineralization associated with these rocks is currently poorly understood.
Rongtu Ma +3 more
semanticscholar +1 more source
Mineralogical magazine, 2021
The Neoproterozoic Lofdal alkaline carbonatite complex consists of a swarm of carbonatite dykes and two plugs of calcite carbonatite known as the ‘Main’ and ‘Emanya’ carbonatite intrusions, with associated dykes and plugs of phonolite, syenite, rare ...
M. Sitnikova +3 more
semanticscholar +1 more source
The Neoproterozoic Lofdal alkaline carbonatite complex consists of a swarm of carbonatite dykes and two plugs of calcite carbonatite known as the ‘Main’ and ‘Emanya’ carbonatite intrusions, with associated dykes and plugs of phonolite, syenite, rare ...
M. Sitnikova +3 more
semanticscholar +1 more source
A common origin of carbonatite magmas
The more than 500 fossil Ca-carbonatite occurrences on Earth are at odds with the only active East African Rift carbonatite volcano, Oldoinyo Lengai (Tanzania), which produces Na-carbonatite magmas.
Daniel Weidendorfer +2 more
exaly +2 more sources
CARBONATITES AND CARBONATITES AND CARBONATITES
The Canadian Mineralogist, 2005Le clan des carbonatites est ici redefini dans le contexte d'une classification mineralogique et genetique, et subdivise en deux groupes: carbonatites primaires et residus carbothermaux. On souligne le fait que "carbonatite" est a la fois un terme petrographique applicable a un type de roche particulier, et un terme faisant reference a un groupe de ...
openaire +1 more source
Economic Geology
The giant Bayan Obo deposit in China represents the largest rare earth element (REE) resource in the world, but the mechanisms for its highly anomalous REE enrichment have long been controversial.
Xiaochun Li +5 more
semanticscholar +1 more source
The giant Bayan Obo deposit in China represents the largest rare earth element (REE) resource in the world, but the mechanisms for its highly anomalous REE enrichment have long been controversial.
Xiaochun Li +5 more
semanticscholar +1 more source
The Primary Geology of the Paleoproterozoic MT Weld Carbonatite Complex, Western Australia
Journal of PetrologyThe paleoregolith overlying the c. 2.06 Ga Mt Weld carbonatite (eastern Yilgarn Craton, Western Australia) hosts one of the largest Rare Earth Element (REE) deposits globally.
Ross Chandler +5 more
semanticscholar +1 more source
Mineralogical magazine, 2021
Pyrochlore-group minerals are common in the Neoproterozoic Sevattur carbonatite complex. This complex is composed of dolomite-, calcite-, banded- and blue carbonatite together with pyroxenite, albitite and diverse syenites.
Monojit Dey +6 more
semanticscholar +1 more source
Pyrochlore-group minerals are common in the Neoproterozoic Sevattur carbonatite complex. This complex is composed of dolomite-, calcite-, banded- and blue carbonatite together with pyroxenite, albitite and diverse syenites.
Monojit Dey +6 more
semanticscholar +1 more source

